Dune Sediments

The Namib Sand Sea, characterized by its yellowish brown to yellowish red quartz sand, offers critical insights into the sedimentary processes shaping one of Earth's largest dune fields. This study reveals that the sediments within and between dunes are a direct product of ongoing accumulation, providing a geological record of the sand sea's development. By analyzing these sediments, researchers can reconstruct the dynamic interactions between wind, sand transport, and deposition over time. The research employs a combination of field observations, sediment analysis, and geomorphological mapping to unravel the complex history of this unique desert landscape.

Lancaster, N. (2026). Dune Sediments. The Namib Sand Sea, 47–80. https://doi.org/10.1201/9781003763185-4